User:Skaleka

[http://en.wikibooks.org/w/index.php?title=User:Skaleka&action=edit The difference in the origin of igneous, sedimentary, and metamorphic rocks vary of how they feel, how they are shaped, and even what color they may be. Igneous rocks are solidified directly from molten silicates and examples of this are granite and basalt. Sedimentary rocks are formed when igneous rocks eroded as sediment under the sea and examples of this are limestone and sandstone. Metamorphic rocks are comprised of both igneous and sedimentary rocks of all ages which are which have been gone under intense pressure and examples of this are slate and marble. Gypsum: File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011 2/Photo on 2011-01-05 at 13.16.jpg File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011 3/-drywall-inspection.jpg Quartz: File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011 4/Photo on 2011-01-05 at 13.05 File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011 5/-laptop.jpg Feldspar: File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011 7/Photo on 2011-01-05 at 14.39.jpg File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011 8/BonAmiLOWRESWhiteBkg.gif Geode: BEFORE- [[File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011_10/Photo on 2011-01-05 at 14.54.jpg ] AFTER- File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011 9/Photo on 2011-01-05 at 15.00.jpg They are found in the Midwest and with Wisconsin being in the Midwest, it is a possibility that it be found in rural areas. ]The difference in the origin of igneous, sedimentary, and metamorphic rocks vary of how they feel, how they are shaped, and even what color they may be. Igneous rocks are solidified directly from molten silicates and examples of this are granite and basalt. Sedimentary rocks are formed when igneous rocks eroded as a sediment under the sea and examples of this are limestone and sandstone. Metamorphic rocks are comprised of both igneous and sedimentary rocks of all ages which are which have been gone under intense pressure and examples of this are slate and marble. Gypsum: [[File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011_2/Photo on 2011-01-05 at 13.16.jpg]]



Quartz:



Feldspar:



Geode: BEFORE- [[File:/Users/Simran/Pictures/iPhoto Library/Originals/2011/Jan 5, 2011_10/Photo on 2011-01-05 at 14.54.jpg]

AFTER-

They are found in the Midwest and with Wisconsin being in the Midwest, it is a possibility that it be found in rural areas.